That's right, Mozz, and by the way I was just joking . Feel free to jump in any time.

Grendel raised an interesting point about volcanoes. Let's examine that.
If we look at the graph of mean global temperature, we can see a small blip about 18 months after the eruption of Mt Pinatabo in 1991. The interesting thing is that the blip is in the
negative, and that's because explosive stratospheric volcanoes like Mt Pinatabo release primarily dust and sulphur dioxide which have an overall cooling effect. You can discount virtually all volcanoes beneath the sea, because almost without exception, they are basaltic, and have very little gas evolution. The ones that make the difference are very large stratospheric volcanoes.
Gases and dust from stratospheric volcanoes are carried up into the stratosphere (12 to 15 km above the ground). There, because this is well above the clouds and rain of the troposphere, the sulphates can hang around for a long time (sometimes a few years).
Prior to that El Chichon (Mexico, in 1982), Mt. Agung (Indonesia, 1963), Santa Maria (Guatemala, 1902) and Krakatoa (Indonesia, 1883) all had noticeable cooling effects. There was quite a large volcano in Chile last year, but that is not expected to have any significant cooling effect. The main reason is that it was too far from the equator, and was too small to have any appreciable effect.